The Deep Roots of the Rocky Mountains: Geophysical Studies of Western Canada
Author(s) -
Claire A. Currie
Publication year - 2016
Publication title -
journal of student science and technology
Language(s) - English
Resource type - Journals
eISSN - 2291-6954
pISSN - 1913-1925
DOI - 10.13034/jsst.v9i1.142
Subject(s) - geology , snow , tectonics , terrain , western europe , physical geography , mountain range (options) , geomorphology , archaeology , geography , paleontology , cartography , european union , economics , financial economics , business , economic policy
The Rocky Mountains in western Canada have some of the most spectacular scenery in the world, with rugged terrain and snow-covered peaks. The Rockies are part of the North American Cordillera, a ~4000 km mountain belt that runs along the western side of North America (Figure 1). This mountain belt formed over the last 200 million years, as rocks were added to the western side of North America during the convergence of tectonic plates.
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